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On February 27, 2007 a new eruption started at Stromboli that lasted until April 2 and included a paroxysmal
12 explosion on March 15. Geochemical monitoring carried out over several years revealed some appreciable
13 variations that preceded both the eruption onset and the explosion. The carbon dioxide (CO2) flux from the
14 soil at Pizzo Sopra La Fossa increased markedly a few days before the eruption onset, and continued during
15 lava effusion to reach its maximum value (at 90,000 g m−2 day−1) a few days before the paroxysm. Almost
16 contemporarily, the δ13CCO2 of the SC5 fumarole located in the summit area increased markedly, peaking just
17 before the explosion (δ13CCO2~−1.8‰). Following the paroxysm, helium (He) isotopes measured in the gases
18 dissolved in the basal thermal aquifer sharply increased. Almost contemporarily, the automatic station of CO2
19 flux recorded an anomalous degassing rate. Also temperatures and the vertical thermal gradient, which had
20 been measured since November 2006 in the soil at Pizzo Sopra La Fossa, showed appreciable variabilities that
21 lasted until the end of the eruption. The geochemical variations indicated the degassing of a new batch of
22 volatile-rich magma that preceded and probably fed the paroxysm. The anomalous 3He/4He ratio suggested
23 that the ascent of a second batch of volatile-rich magma toward the surface was probably responsible of the
24 resumption of the ordinary activity. A comparison with the geochemical variations observed during the
25 2002–2003 eruption indicated that the 2007 eruption was less energetic.